中国的氦资源和氦游戏分类系统、有效的储层控制要素和富集模式

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引用次数: 0

摘要

从氦气的来源、载体、地质背景、典型富氦气田解剖等方面,分析了中国氦气资源的分类体系、储层有效控制要素、主要富集勘探模式。首先,基于氦气的特殊性和天然气积聚与成藏的相关性分析,从氦气母源、氦气类型多样性、储藏类型和载体类型等九个方面,分析梳理了我国氦气资源及赋存类型划分方案和分类体系、载气的技术经济可采特征、载气成因、载气的主要成分、氦源与储层的匹配组合、盆地结构原型背景、氦含量等九个方面,为后续有针对性地开展不同类别的详细研究和评价方案奠定基础。其次,分析指出了我国东、中、西部氦资源类型的纵横向分布特征、构造动力学特征、地质地球化学特征以及氦矿床形成的关键条件。再次,从氦气 "生成-迁移-富集 "系统和富氦储层形成的控制要素及有效性角度,分析了氦气富集的有效控制要素和地质评价中值得关注的相关问题,指出了氦储层形成和勘探评价中存在的误区。最后,从盆地构造背景、富氦控制机理和勘探方向等方面,提出了中国 "原始盆地-构造-岩性-载气 "氦气聚集四要素组合带的勘探评价方向和分类方案,并据此梳理出中国四类盆地和八类富氦带。在这八种类型的富氦带中,有八种典型的富氦田富集和勘探模式,包括中国古代克拉通隆起型、克拉通边缘断裂-褶皱变型、断裂-隆起型凹陷盆地、斜坡隆起-隆起型前陆盆地、断裂-凸起型断裂盆地、U/Th-富集基底型、U/Th-富集基底型、U/Th-富集基底型、U/Th-富集基底型、U/Th-富集基底型、U/Th-富集基底型、分析了不同类型富氦矿床形成的主要控制因素,为后续类似富氦地区的勘探发现和勘探目标评价提供了参考。
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Helium resource and play classification systems, effective reservoir control elements, and enrichment patterns in China

The classification system, effective reservoir control elements, and major enrichment and exploration modes of helium resources in China are analyzed based on the source of helium, carrier, geological background, and anatomy of typical helium-rich fields. Firstly, based on the special characteristics of helium and the correlation analysis of natural gas accumulation and reservoir formation, we analyzed and sorted out the helium resource and play type classification scheme and classification system in China from nine aspects, namely, the source of helium parental sources, helium type diversities, the storage and carrier types, the technically and economically recoverable characteristics of carrier gases, the carrier gas genesis, the main components of carrier gases, the matching combination of helium sources and reservoirs, background of prototype basin structure, and helium content, to lay the foundation for the subsequent targeted and detailed studies and evaluation programs in different categories. Secondly, the analysis points out the characteristics of helium resource types in the east, middle, and west of China in terms of longitudinal and transverse distribution, tectonic dynamics, geological and geochemical characteristics, and key conditions for the formation of helium deposits. Thirdly, from the perspective of the helium “generation-migration-accumulation” system and the controlling elements and effectiveness of helium-rich reservoir formation, we analyze the effective controlling elements of helium accumulation and the related problems that deserve attention in geological evaluation and point out the misunderstandings in helium reservoir formation and exploration evaluation. Last but not least, from the perspective of basin tectonic background, helium enrichment controlling mechanism and exploration direction, the exploration and evaluation direction and classification scheme for the four element combination zones of “original basin–structure–lithology–carrier gas” helium accumulation in China have been proposed, based on which, four types of basins and eight types of helium-rich zones in China have been sorted out. In these eight types of helium-rich zones, eight typical helium-rich field enrichment and exploration patterns, including the ancient uplift type of China's craton, fracture-fold variant of the craton margin, fracture-rise type of depression basin, slope bulge and uplift type of foreland basin, fracture-convex type of fracture basin, and U/Th-rich basement type of basin were analyzed, and the main controlling factors of the formation of different types of helium-rich deposits were analyzed, which will provide a reference for the subsequent exploration and discovery of similar helium-rich areas and exploration target evaluation.

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